untitled
<OAI-PMH schemaLocation=http://www.openarchives.org/OAI/2.0/ http://www.openarchives.org/OAI/2.0/OAI-PMH.xsd>
<responseDate>2018-01-15T18:19:39Z</responseDate>
<request identifier=oai:HAL:hal-01426582v1 verb=GetRecord metadataPrefix=oai_dc>http://api.archives-ouvertes.fr/oai/hal/</request>
<GetRecord>
<record>
<header>
<identifier>oai:HAL:hal-01426582v1</identifier>
<datestamp>2018-01-11</datestamp>
<setSpec>type:COMM</setSpec>
<setSpec>subject:sdu</setSpec>
<setSpec>subject:phys</setSpec>
<setSpec>collection:CNRS</setSpec>
<setSpec>collection:UNIV-AG</setSpec>
<setSpec>collection:UNIV-TLN</setSpec>
<setSpec>collection:GM</setSpec>
<setSpec>collection:OSU-INSTITUT-PYTHEAS</setSpec>
<setSpec>collection:CEREGE</setSpec>
<setSpec>collection:CDF</setSpec>
<setSpec>collection:AGROPOLIS</setSpec>
<setSpec>collection:UNIV-AMU</setSpec>
<setSpec>collection:GIP-BE</setSpec>
<setSpec>collection:INSU</setSpec>
<setSpec>collection:PSL</setSpec>
<setSpec>collection:MIO</setSpec>
<setSpec>collection:B3ESTE</setSpec>
<setSpec>collection:UNIV-MONTPELLIER</setSpec>
</header>
<metadata><dc>
<publisher>HAL CCSD</publisher>
<title lang=en>The structure of nearshore currents driven by changes in meteo-marine forcings</title>
<creator>Petitjean, Lise</creator>
<creator>Sous, Damien</creator>
<creator>Rey, Vincent</creator>
<creator>BOUCHETTE, Frederic</creator>
<creator>Sabatier, Francois</creator>
<creator>Meulé, Samuel</creator>
<contributor>Institut méditerranéen d'océanologie (MIO) ; Institut de Recherche pour le Développement (IRD) - Aix Marseille Université (AMU) - Institut de recherche pour le développement [IRD] : UMR235 - Université de Toulon (UTLN) - Centre National de la Recherche Scientifique (CNRS)</contributor>
<contributor>Géosciences Montpellier ; Université des Antilles et de la Guyane (UAG) - Institut national des sciences de l'Univers (INSU - CNRS) - Université de Montpellier (UM) - Centre National de la Recherche Scientifique (CNRS)</contributor>
<contributor>Centre européen de recherche et d'enseignement de géosciences de l'environnement (CEREGE) ; Institut de Recherche pour le Développement (IRD) - Aix Marseille Université (AMU) - Collège de France (CdF) - Institut national des sciences de l'Univers (INSU - CNRS) - Centre National de la Recherche Scientifique (CNRS)</contributor>
<description>International audience</description>
<source>35th International Conference on Coastal Engineering</source>
<coverage>Antalya, Turkey</coverage>
<identifier>hal-01426582</identifier>
<identifier>https://hal.archives-ouvertes.fr/hal-01426582</identifier>
<source>https://hal.archives-ouvertes.fr/hal-01426582</source>
<source>35th International Conference on Coastal Engineering, Nov 2016, Antalya, Turkey. 2016, 〈http://icce2016.com〉</source>
<source>http://icce2016.com</source>
<language>en</language>
<subject lang=en>nearshore circulation</subject>
<subject lang=en> microtidal barred beach</subject>
<subject lang=en> vertical velocity structure</subject>
<subject>[SDU.STU.GM] Sciences of the Universe [physics]/Earth Sciences/Geomorphology</subject>
<subject>[PHYS] Physics [physics]</subject>
<subject>[SDU.STU.OC] Sciences of the Universe [physics]/Earth Sciences/Oceanography</subject>
<type>info:eu-repo/semantics/conferenceObject</type>
<type>Conference papers</type>
<description lang=en>This work aims to better understand the physical processes governing the wave propagation in a vertically shearedcurrent and the resulting nearshore circulation patterns. It is based on a high resolution hydro-morphodynamic fieldcampaign, ROUSTY2014, collecting a comprehensive hydro-morphodynamical dataset during a full winter season.The overall analysis highlights three main circulation patterns, largely controled by the bathymetric features and byco-working or competing wind and waves forcings. Regarding the vertical structuration of the circulation, most of fieldobservations shown seaward directed circulation with onshore component close to the air/sea surface whose intensityvaries according to incoming wave conditions. Forth, vertical shear increase when breaking happen close to sensorlocation and orientation of mean circulation depend on wind direction.</description>
<date>2016-11-17</date>
</dc>
</metadata>
</record>
</GetRecord>
</OAI-PMH>
